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Evolution of Soils on Quaternary Reef Terraces of Barbados, West Indies

Published online by Cambridge University Press:  20 January 2017

Daniel R. Muhs
Affiliation:
U.S. Geological Survey, MS 980, Federal Center, Box 25046, Denver, Colorado, 80225

Abstract

Soils on uplifted Quaternary reef terraces of Barbados, ∼125,000 to ∼700,000 yr old, form a climo-chronosequence and show changes in physical, chemical, and mineralogical properties with terrace age. Parent materials are dust derived from the Sahara, volcanic ash from the Lesser Antilles island arc, and detrital carbonate from the underlying reef limestone. Although some terrace soils are probably eroded, soils or their remnants are redder and more clay-rich with increasing terrace age. Profile-average Al2O3 and Fe2O3 content increases with terrace age, which partially reflects the increasing clay content, but dithionite-extractable Fe also increases with terrace age. Profile-average K2O/TiO2, Na2O/TiO2, and P2O5/TiO2 values decrease with terrace age, reflecting the depletion of primary minerals. Average SiO2/Al2O3 values also decrease with terrace age and reflect not only loss of primary minerals but also evolution of secondary clay minerals. Although they are not present in any of the parent materials, the youngest terrace soils are dominated by smectite and interstratified kaolinite-smectite, which gradually alter to relatively pure kaolinite over ∼700,000 yr. Comparisons with other tropical islands, where precipitation is higher and rates of dust fall may be lower, show that Barbados soils are less weathered than soils of comparable age. It is concluded that many soil properties in tropical regions can be potentially useful relative-age indicators in Quaternary stratigraphic studies, even when soils are eroded or changes in soil morphology are not dramatic.

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Research Article
Copyright
University of Washington

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References

Acker, K.L., and Stearn, C.W. (1969). Carbonate-siliciclastic facies transition and reef growth on the northeast coast of Barbados, West Indies. Journal of Sedimentary Petrology 60, 1825.Google Scholar
Ahmad, N., and Jones, R.L. (1983). Genesis, chemical properties and mineralogy of limestone-derived soils, Barbados, West Indies. Tropical Agriculture 46, 115.Google Scholar
Alexander, E.B., and Holowaychuk, N. (1979). Soils on terraces along the Cauca River, Colombia; I, Chronosequence characteristics. Soil Science Society of America Journal 47, 715721.CrossRefGoogle Scholar
Bender, M.L., Fairbanks, R.G., Taylor, F.W., Matthews, R.K., Goddard, J.G., and Broecker, W.S. (1999). Uranium-series dating of the Pleistocene reef tracts of Barbados, West Indies. Geological Society of America Bulletin, Part I 90, 557594.Google Scholar
Birkeland, P.W. (1996). Soils and Geomorphology. Oxford Univ. Press, London.Google Scholar
Borg, L.E., and Banner, J.L. (1980). Neodymium and strontium isotopic constraints on soil sources in Barbados, West Indies. Geochimica et Cosmochimica Acta 60, 41934206.CrossRefGoogle Scholar
Brindley, G.W., and Brown, G. (1972). Crystal Structures of Clay Minerals and Their X-ray Identification. Mineralogical Society Monograph No. 5, London.Google Scholar
Carroll, D, and Hathaway, J. C. Mineralogy of Selected Soils from Guam. U.S. Geological Survey Professional Paper 403-F.Google Scholar
Cradwick, P.D., and Wilson, M.J. (1995). Calculated X-ray diffraction profiles for interstratified kaolinite-montmorillonite. Clay Minerals 9, 395405.CrossRefGoogle Scholar
Davis, R.A. Jr. (1967). Geologic impact of Hurricane Andrew on Everglades coast of southwest Florida. Environmental Geology 25, 143148.CrossRefGoogle Scholar
Delany, A.C., Delany, A.C., Parkin, D.W., Griffin, J.J., Goldberg, E.D., and Reimann, B.E.F. (1997). Airborne dust collected at Barbados. Geochimica et Cosmochimica Acta 31, 885909.CrossRefGoogle Scholar
Edwards, R.L., Cheng, H., Murrell, M.T., and Goldstein, S.J. (1991). Protactinium-231 dating of carbonates by thermal ionization mass spectrometry: Implications for Quaternary climate change. Science 276, 782786.CrossRefGoogle ScholarPubMed
Foos, A.M. (2000). Aluminous lateritic soils, Eleuthera, Bahamas: A modern analog to carbonate paleosols. Journal of Sedimentary Petrology 61, 340348.Google Scholar
Fruijtier, C., Elliott, T., and Schlager, W. (1994). Mass-spectrometric 234U-230Th ages from the Key Largo Formation, Florida Keys, United States: Constraints on diagenetic age disturbance. Geological Society of America Bulletin 112, 267277.2.0.CO;2>CrossRefGoogle Scholar
Gallup, C.D., Edwards, R.L., and Johnson, R.G. (1979). The timing of high sea levels over the past 200,000 years. Science 263, 796800.CrossRefGoogle ScholarPubMed
Geiger, L., and Nettleton, W.D. (1978). Properties and geomorphic relationships of some soils of Liberia. Soil Science Society of America Journal 43, 11921198.CrossRefGoogle Scholar
Glaccum, R.A. (1980). The Mineralogy and Elemental Composition of Mineral Aerosols over the Tropical North Atlantic: The Influence of Saharan Dust. University of Miami, Google Scholar
Glaccum, R.A., and Prospero, J.M. (1993). Saharan aerosols over the tropical North Atlantic—Mineralogy. Marine Geology 37, 295321.CrossRefGoogle Scholar
Goldich, S. S, and Bergquist, H. R. Aluminous Lateritic Soil of the Republic of Haiti. W.I. U.S. Geological Survey Bulletin 954-C.Google Scholar
Goodfriend, G.A., and Mitterer, R.M. (1994). A 45,000-yr record of a tropical lowland biota: The land snail fauna from cave sediments at Coco Ree, Jamaica. Geological Society of America Bulletin 105, 1829.2.3.CO;2>CrossRefGoogle Scholar
Guilderson, T.P., Fairbanks, R.G., and Rubenstone, J.L. (1977). Tropical temperature variations since 20,000 years ago: Modulating interhemispheric climate change. Science 263, 663665.CrossRefGoogle ScholarPubMed
Harrison, R.S. (1998). Caliche profiles: Indicators of near-surface subaerial diagenesis, Barbados, West Indies. Bulletin of Canadian Petroleum Geology 25, 123173.Google Scholar
Heath, E., MacDonald, R., Belkin, H., Hawkesworth, C., and Sigurdsson, H. (1965). Magmagenesis at Soufriere volcano, St Vincent, Lesser Antilles arc. Journal of Petrology 39, 17211764.CrossRefGoogle Scholar
Herwitz, S.R., and Muhs, D.R. (1966). Bermuda solution pipe soils: A geochemical evaluation of eolian parent materials. Curran, H.A., and White, B. (1995). Terrestrial and Shallow Marine Geology of the Bahamas and Bermuda. 311323.Google Scholar
Herwitz, S.R., Muhs, D.R., Prospero, J.M., Mahan, S., and Vaughn, B. (1996). Origin of Bermuda's clay-rich Quaternary paleosols and their paleoclimatic significance. Journal of Geophysical Research 101, 23,38923,400.CrossRefGoogle Scholar
Holmes, J.A., Street-Perrott, F.A., Ivanovich, M., and Perrott, R.A. (1995). A late Quaternary palaeolimnological record from Jamaica based on trace-element chemistry of ostracod shells. Chemical Geology 124, 143160.CrossRefGoogle Scholar
Lepsch, I.F., Buol, S.W., and Daniels, R.B. (1977). Soil landscape relationships in the Occidental Plateau of Sao Paulo State, Brazil; II, Soil morphology, genesis, and classification. Soil Science Society of America Journal 41, 109115.CrossRefGoogle Scholar
Mesolella, K.J., Matthews, R.K., Broecker, W.S., and Thurber, D.L. (1969). The astronomical theory of climatic change: Barbados data. Journal of Geology 77, 250274.CrossRefGoogle Scholar
Muhs, D.R., Bettis, E.A. III (2000). Geochemical variations in Peoria Loess of western Iowa indicate paleowinds of midcontinental North America during last glaciation. Quaternary Research 53, 4961.CrossRefGoogle Scholar
Muhs, D.R., Crittenden, R.C., Rosholt, J.N., Bush, C.A., and Stewart, K.C. (1987). Genesis of marine terrace soils, Barbados, West Indies: Evidence from mineralogy and geochemistry. Earth Surface Processes and Landforms 12, 605618.CrossRefGoogle Scholar
Muhs, D.R., Bush, C.A., Stewart, K.C., Rowland, T.R., and Crittenden, R.C. (1990). Geochemical evidence of Saharan dust parent material for soils developed on Quaternary limestones of Caribbean and western Atlantic islands. Quaternary Research 33, 157177.CrossRefGoogle Scholar
Nieuwenhuyse, A., and van Breeman, N. (1997). Quantitative aspects of weathering and neoformation in selected Costa Rican volcanic soils. Soil Science Society of America Journal 61, 14501458.CrossRefGoogle Scholar
Prospero, J.M. (1981). Arid regions as sources of mineral aerosols in the marine atmosphere. Geological Society of America Special Paper 186, 7186.CrossRefGoogle Scholar
Prospero, J.M., Bonatti, E., Schubert, C., and Carlson, T.N. (1970). Dust in the Caribbean atmosphere traced to an African dust storm. Earth and Planetary Science Letters 9, 287293.CrossRefGoogle Scholar
Radtke, U., Grün, R., and Schwarcz, H.P. (1988). Electron spin resonance dating of the Pleistocene coral reef tracts of Barbados. Quaternary Research 29, 197215.CrossRefGoogle Scholar
Rouse, W. R, and Watts, D. Two studies in Barbadian Climatology. Climatological Research Series No. 1, McGill University, Montreal., 119, pp.Google Scholar
Schaetzl, R.J., Barrett, L.R., and Winkler, J.A. (1994). Choosing models for soil chronofunctions and fitting them to data. European Journal of Soil Science 45, 219232.CrossRefGoogle Scholar
Vernon, K. C., and Carroll, D. M. “Barbados”. Soil and Land-Use Surveys 18 , Regional Research Centre, University of the West Indies, Trinidad.Google Scholar
Vitousek, P.M., Chadwick, O.M., Crews, T.E., Fownes, J.H., Hendricks, D.M., and Herbert, D. (1997). Soil and ecosystem development across the Hawaiian Islands. GSA Today 7, 18.Google Scholar
Walker, T.W., and Syers, J.K. (1976). The fate of phosphorus during pedogenesis. Geoderma 15, 119.CrossRefGoogle Scholar
Watts, D. (1970). Persistence and change in the vegetation of oceanic islands: An example from Barbados, West Indies. Canadian Geographer 14, 91109.CrossRefGoogle Scholar
Watts, W.A., and Hansen, B.C.S. (1994). Pre-Holocene and Holocene pollen records of vegetation history from the Florida peninsula and their climatic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 109, 163176.CrossRefGoogle Scholar
Weaver, C.E., and Pollard, L.D. (1973). The Chemistry of Clay Minerals. Elsevier Scientific Publishing Company, New York.Google ScholarPubMed

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